[2089] | 1 | !****************************************************************************** |
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| 2 | ! * |
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| 3 | ! Optical depths developed for the * |
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| 4 | ! * |
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| 5 | ! RAPID RADIATIVE TRANSFER MODEL (RRTM) * |
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| 6 | ! * |
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| 7 | ! ATMOSPHERIC AND ENVIRONMENTAL RESEARCH, INC. * |
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| 8 | ! 840 MEMORIAL DRIVE * |
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| 9 | ! CAMBRIDGE, MA 02139 * |
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| 10 | ! * |
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| 11 | ! ELI J. MLAWER * |
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| 12 | ! STEVEN J. TAUBMAN * |
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| 13 | ! SHEPARD A. CLOUGH * |
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| 14 | ! * |
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| 15 | ! email: mlawer@aer.com * |
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| 16 | ! * |
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| 17 | ! The authors wish to acknowledge the contributions of the * |
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| 18 | ! following people: Patrick D. Brown, Michael J. Iacono, * |
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| 19 | ! Ronald E. Farren, Luke Chen, Robert Bergstrom. * |
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| 20 | ! * |
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| 21 | !****************************************************************************** |
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| 22 | ! Modified by: * |
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| 23 | ! JJ Morcrette 980714 ECMWF for use on ECMWF's Fujitsu VPP770 * |
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| 24 | ! Reformatted for F90 by JJMorcrette, ECMWF * |
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| 25 | ! - replacing COMMONs by MODULEs * |
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| 26 | ! - changing labelled to unlabelled DO loops * |
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| 27 | ! - creating set-up routines for all block data statements * |
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| 28 | ! - reorganizing the parameter statements * |
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| 29 | ! - passing KLEV as argument * |
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| 30 | ! - suppressing some equivalencing * |
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| 31 | ! * |
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| 32 | ! D Salmond 9907 ECMWF Speed-up modifications * |
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| 33 | ! D Salmond 000515 ECMWF Speed-up modifications * |
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| 34 | !****************************************************************************** |
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| 35 | ! TAUMOL * |
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| 36 | ! * |
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| 37 | ! This file contains the subroutines TAUGBn (where n goes from * |
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| 38 | ! 1 to 16). TAUGBn calculates the optical depths and Planck fractions * |
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| 39 | ! per g-value and layer for band n. * |
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| 40 | ! * |
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| 41 | ! Output: optical depths (unitless) * |
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| 42 | ! fractions needed to compute Planck functions at every layer * |
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| 43 | ! and g-value * |
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| 44 | ! * |
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| 45 | ! COMMON /TAUGCOM/ TAUG(MXLAY,MG) * |
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| 46 | ! COMMON /PLANKG/ FRACS(MXLAY,MG) * |
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| 47 | ! * |
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| 48 | ! Input * |
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| 49 | ! * |
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| 50 | ! COMMON /FEATURES/ NG(NBANDS),NSPA(NBANDS),NSPB(NBANDS) * |
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| 51 | ! COMMON /PRECISE/ ONEMINUS * |
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| 52 | ! COMMON /PROFILE/ NLAYERS,PAVEL(MXLAY),TAVEL(MXLAY), * |
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| 53 | ! & PZ(0:MXLAY),TZ(0:MXLAY),TBOUND * |
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| 54 | ! COMMON /PROFDATA/ LAYTROP,LAYSWTCH,LAYLOW, * |
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| 55 | ! & COLH2O(MXLAY),COLCO2(MXLAY), * |
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| 56 | ! & COLO3(MXLAY),COLN2O(MXLAY),COLCH4(MXLAY), * |
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| 57 | ! & COLO2(MXLAY),CO2MULT(MXLAY) * |
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| 58 | ! COMMON /INTFAC/ FAC00(MXLAY),FAC01(MXLAY), * |
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| 59 | ! & FAC10(MXLAY),FAC11(MXLAY) * |
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| 60 | ! COMMON /INTIND/ JP(MXLAY),JT(MXLAY),JT1(MXLAY) * |
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| 61 | ! COMMON /SELF/ SELFFAC(MXLAY), SELFFRAC(MXLAY), INDSELF(MXLAY) * |
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| 62 | ! * |
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| 63 | ! Description: * |
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| 64 | ! NG(IBAND) - number of g-values in band IBAND * |
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| 65 | ! NSPA(IBAND) - for the lower atmosphere, the number of reference * |
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| 66 | ! atmospheres that are stored for band IBAND per * |
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| 67 | ! pressure level and temperature. Each of these * |
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| 68 | ! atmospheres has different relative amounts of the * |
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| 69 | ! key species for the band (i.e. different binary * |
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| 70 | ! species parameters). * |
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| 71 | ! NSPB(IBAND) - same for upper atmosphere * |
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| 72 | ! ONEMINUS - since problems are caused in some cases by interpolation * |
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| 73 | ! parameters equal to or greater than 1, for these cases * |
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| 74 | ! these parameters are set to this value, slightly < 1. * |
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| 75 | ! PAVEL - layer pressures (mb) * |
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| 76 | ! TAVEL - layer temperatures (degrees K) * |
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| 77 | ! PZ - level pressures (mb) * |
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| 78 | ! TZ - level temperatures (degrees K) * |
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| 79 | ! LAYTROP - layer at which switch is made from one combination of * |
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| 80 | ! key species to another * |
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| 81 | ! COLH2O, COLCO2, COLO3, COLN2O, COLCH4 - column amounts of water * |
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| 82 | ! vapor,carbon dioxide, ozone, nitrous ozide, methane, * |
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| 83 | ! respectively (molecules/cm**2) * |
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| 84 | ! CO2MULT - for bands in which carbon dioxide is implemented as a * |
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| 85 | ! trace species, this is the factor used to multiply the * |
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| 86 | ! band's average CO2 absorption coefficient to get the added * |
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| 87 | ! contribution to the optical depth relative to 355 ppm. * |
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| 88 | ! FACij(LAY) - for layer LAY, these are factors that are needed to * |
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| 89 | ! compute the interpolation factors that multiply the * |
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| 90 | ! appropriate reference k-values. A value of 0 (1) for * |
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| 91 | ! i,j indicates that the corresponding factor multiplies * |
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| 92 | ! reference k-value for the lower (higher) of the two * |
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| 93 | ! appropriate temperatures, and altitudes, respectively. * |
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| 94 | ! JP - the index of the lower (in altitude) of the two appropriate * |
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| 95 | ! reference pressure levels needed for interpolation * |
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| 96 | ! JT, JT1 - the indices of the lower of the two appropriate reference * |
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| 97 | ! temperatures needed for interpolation (for pressure * |
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| 98 | ! levels JP and JP+1, respectively) * |
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| 99 | ! SELFFAC - scale factor needed to water vapor self-continuum, equals * |
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| 100 | ! (water vapor density)/(atmospheric density at 296K and * |
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| 101 | ! 1013 mb) * |
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| 102 | ! SELFFRAC - factor needed for temperature interpolation of reference * |
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| 103 | ! water vapor self-continuum data * |
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| 104 | ! INDSELF - index of the lower of the two appropriate reference * |
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| 105 | ! temperatures needed for the self-continuum interpolation * |
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| 106 | ! * |
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| 107 | ! Data input * |
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| 108 | ! COMMON /Kn/ KA(NSPA(n),5,13,MG), KB(NSPB(n),5,13:59,MG), SELFREF(10,MG) * |
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| 109 | ! (note: n is the band number) * |
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| 110 | ! * |
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| 111 | ! Description: * |
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| 112 | ! KA - k-values for low reference atmospheres (no water vapor * |
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| 113 | ! self-continuum) (units: cm**2/molecule) * |
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| 114 | ! KB - k-values for high reference atmospheres (all sources) * |
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| 115 | ! (units: cm**2/molecule) * |
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| 116 | ! SELFREF - k-values for water vapor self-continuum for reference * |
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| 117 | ! atmospheres (used below LAYTROP) * |
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| 118 | ! (units: cm**2/molecule) * |
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| 119 | ! * |
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| 120 | ! DIMENSION ABSA(65*NSPA(n),MG), ABSB(235*NSPB(n),MG) * |
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| 121 | ! EQUIVALENCE (KA,ABSA),(KB,ABSB) * |
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| 122 | ! * |
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| 123 | !****************************************************************************** |
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| 124 | |
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| 125 | |
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| 126 | SUBROUTINE RRTM_TAUMOL1 (KLEV,TAU,& |
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| 127 | &TAUAERL,FAC00,FAC01,FAC10,FAC11,FORFAC,JP,JT,JT1,& |
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| 128 | &COLH2O,LAYTROP,SELFFAC,SELFFRAC,INDSELF,PFRAC) |
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| 129 | |
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| 130 | ! Written by Eli J. Mlawer, Atmospheric & Environmental Research. |
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| 131 | ! Revised by Michael J. Iacono, Atmospheric & Environmental Research. |
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| 132 | |
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| 133 | ! BAND 1: 10-250 cm-1 (low - H2O; high - H2O) |
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| 134 | |
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| 135 | ! Modifications |
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| 136 | ! |
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| 137 | ! D Salmond 2000-05-15 speed-up |
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| 138 | ! JJMorcrette 2000-05-17 speed-up |
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| 139 | |
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| 140 | |
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| 141 | #include "tsmbkind.h" |
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| 142 | |
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| 143 | USE PARRRTM , ONLY : JPLAY ,JPBAND ,JPGPT ,JPXSEC |
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| 144 | USE YOERRTWN , ONLY : NG ,NSPA ,NSPB |
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| 145 | USE YOERRTA1 , ONLY : NG1 ,ABSA ,ABSB ,FRACREFA, FRACREFB,& |
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| 146 | &FORREF ,KA ,KB ,SELFREF |
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| 147 | |
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| 148 | !#include "yoeratm.h" |
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| 149 | |
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| 150 | ! REAL TAUAER(JPLAY) |
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| 151 | |
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| 152 | IMPLICIT NONE |
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| 153 | |
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| 154 | ! Output |
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| 155 | REAL_B :: TAU (JPGPT,JPLAY) |
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| 156 | |
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| 157 | ! DUMMY INTEGER SCALARS |
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| 158 | INTEGER_M :: KLEV |
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| 159 | |
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| 160 | !- from AER |
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| 161 | REAL_B :: TAUAERL(JPLAY,JPBAND) |
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| 162 | |
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| 163 | !- from INTFAC |
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| 164 | REAL_B :: FAC00(JPLAY) |
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| 165 | REAL_B :: FAC01(JPLAY) |
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| 166 | REAL_B :: FAC10(JPLAY) |
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| 167 | REAL_B :: FAC11(JPLAY) |
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| 168 | REAL_B :: FORFAC(JPLAY) |
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| 169 | |
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| 170 | !- from INTIND |
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| 171 | INTEGER_M :: JP(JPLAY) |
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| 172 | INTEGER_M :: JT(JPLAY) |
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| 173 | INTEGER_M :: JT1(JPLAY) |
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| 174 | |
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| 175 | !- from PRECISE |
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| 176 | REAL_B :: ONEMINUS |
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| 177 | |
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| 178 | !- from PROFDATA |
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| 179 | REAL_B :: COLH2O(JPLAY) |
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| 180 | INTEGER_M :: LAYTROP |
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| 181 | |
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| 182 | !- from SELF |
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| 183 | REAL_B :: SELFFAC(JPLAY) |
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| 184 | REAL_B :: SELFFRAC(JPLAY) |
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| 185 | INTEGER_M :: INDSELF(JPLAY) |
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| 186 | |
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| 187 | !- from SP |
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| 188 | REAL_B :: PFRAC(JPGPT,JPLAY) |
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| 189 | |
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| 190 | INTEGER_M :: IND0(JPLAY),IND1(JPLAY),INDS(JPLAY) |
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| 191 | |
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| 192 | ! LOCAL INTEGER SCALARS |
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| 193 | INTEGER_M :: IG, LAY |
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| 194 | |
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| 195 | ! EQUIVALENCE (TAUAERL(1,1),TAUAER) |
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| 196 | |
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| 197 | ! Compute the optical depth by interpolating in ln(pressure) and |
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| 198 | ! temperature. Below LAYTROP, the water vapor self-continuum |
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| 199 | ! is interpolated (in temperature) separately. |
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| 200 | |
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| 201 | DO LAY = 1, LAYTROP |
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| 202 | IND0(LAY) = ((JP(LAY)-1)*5+(JT(LAY)-1))*NSPA(1) + 1 |
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| 203 | IND1(LAY) = (JP(LAY)*5+(JT1(LAY)-1))*NSPA(1) + 1 |
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| 204 | INDS(LAY) = INDSELF(LAY) |
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| 205 | ENDDO |
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| 206 | |
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| 207 | DO IG = 1, NG1 |
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| 208 | DO LAY = 1, LAYTROP |
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| 209 | !-- DS_000515 |
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| 210 | TAU (IG,LAY) = COLH2O(LAY) *& |
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| 211 | &(FAC00(LAY) * ABSA(IND0(LAY) ,IG) +& |
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| 212 | & FAC10(LAY) * ABSA(IND0(LAY)+1,IG) +& |
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| 213 | & FAC01(LAY) * ABSA(IND1(LAY) ,IG) +& |
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| 214 | & FAC11(LAY) * ABSA(IND1(LAY)+1,IG) +& |
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| 215 | &SELFFAC(LAY) * (SELFREF(INDS(LAY),IG) + & |
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| 216 | &SELFFRAC(LAY) *& |
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| 217 | &(SELFREF(INDS(LAY)+1,IG) - SELFREF(INDS(LAY),IG)))& |
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| 218 | &+ FORFAC(LAY) * FORREF(IG) ) & |
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| 219 | &+ TAUAERL(LAY,1) |
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| 220 | PFRAC(IG,LAY) = FRACREFA(IG) |
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| 221 | ENDDO |
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| 222 | ENDDO |
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| 223 | |
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| 224 | DO LAY = LAYTROP+1, KLEV |
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| 225 | IND0(LAY) = ((JP(LAY)-13)*5+(JT(LAY)-1))*NSPB(1) + 1 |
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| 226 | IND1(LAY) = ((JP(LAY)-12)*5+(JT1(LAY)-1))*NSPB(1) + 1 |
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| 227 | ENDDO |
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| 228 | |
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| 229 | !-- JJM000517 |
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| 230 | DO IG = 1, NG1 |
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| 231 | DO LAY = LAYTROP+1, KLEV |
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| 232 | !-- JJM000517 |
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| 233 | TAU (IG,LAY) = COLH2O(LAY) *& |
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| 234 | &(FAC00(LAY) * ABSB(IND0(LAY) ,IG) +& |
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| 235 | & FAC10(LAY) * ABSB(IND0(LAY)+1,IG) +& |
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| 236 | & FAC01(LAY) * ABSB(IND1(LAY) ,IG) +& |
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| 237 | & FAC11(LAY) * ABSB(IND1(LAY)+1,IG)& |
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| 238 | &+ FORFAC(LAY) * FORREF(IG) ) & |
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| 239 | &+ TAUAERL(LAY,1) |
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| 240 | PFRAC(IG,LAY) = FRACREFB(IG) |
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| 241 | ENDDO |
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| 242 | ENDDO |
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| 243 | |
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| 244 | RETURN |
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| 245 | END SUBROUTINE RRTM_TAUMOL1 |
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